Alignements du Bois de Fourgon — Alignements de menhirs au château de la Guignardière

Stone row (alignment)

Alignements du Bois de Fourgon

France

DatedEst. 3300–2500 BCE

Photo Stephanbloch · Public domainSource file on Wikimedia Commons

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Overview

About this site

Overview

The Alignements du Bois de Fourgon are a group of four megalithic alignments (numbered G1, G2, G2 bis and G3) at Avrillé, in the département of Vendée, France. The catalogue record gives a typological estimate of 3300 to 2500 BCE, and the site lies within a megalithic complex that also includes a dolmen, a megalithic chest, two megalithic quarries and several tumuli.

Excavations by Gérard Benéteau and his team in the 1990s, and again in 2009-2010, revealed further menhirs and alignments. Radiocarbon dates and pottery place the activity in the Middle and Late Neolithic.

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Where it sits in time

The site's dated range, placed against world reference points.

The scale is logarithmic: each step to the left is about ten times older than the last.

Est. 3300–2500 BCEHow this date was established: Type comparisonTypical for this type

What this badge meansThe published range for this kind of monument in this region. It is not a date for this site.
Source for this date

Article

Alignements du Bois de Fourgon

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The complex lies in an enclosed wood, itself part of a former closed estate formed around a Renaissance château, the château de la Guignardière, since the end of the sixteenth century.

Alignements du Bois de Fourgon

Setting

Sources for this section

The complex lies in an enclosed wood, itself part of a former closed estate formed around a Renaissance château, the château de la Guignardière, since the end of the sixteenth century. This setting has probably ensured the good preservation of the megalithic complex.

The site comprises four megalithic alignments oriented north-south, a dolmen, a megalithic chest, two megalithic quarries and several tumuli. One of these is an oval tumulus oriented east-west and surrounded by a ditch, about 12 m long by 6 m wide, situated between groups G1 and G2. The main group stands at the top of the plateau, at an altitude of between 38 m and 47 m.

Description

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Alignment G1 is the easternmost. Before its excavation in 1996 it consisted of a large menhir 6 m high, adjoined by a monolith 2,40 m high and three partly buried blocks, the whole extending over 9 m. After excavation only two overturned blocks in the north were recognised as additional menhirs (numbered 1 and 2). They had been erected in shallow wedging pits 15 cm to 20 cm deep, the wedging stones having been reinforced with a kind of mortar. Menhir no 2 was carefully dressed by bush-hammering to give it an anthropomorphic form. Both menhirs were re-erected after the excavation. A third, triangular block found lying half-way between menhirs 1 and 2 and menhirs 3 and 4 had no corresponding wedging pit. It was therefore not recognised as a menhir but as the remains of an earlier construction, about 2 m by 1 m, which was destroyed when the alignment was built.

Alignment G2 lies 63 m south-west of G1 and consists of five menhirs, four of which were visible before excavation. Pit structures and assembly lines found during the excavation of 1994 were interpreted as traces of the operations by which the large menhir no 3 was raised. The alignment was dismantled in recent times, probably by quarrymen: menhir no 5 was cut up, the visible part corresponding to its top, and menhir no 2 was fractured into three parts, one of which has disappeared. The dismantling may date from the building of the château de la Guignardière, as indicated by fragments of iron tools and a liard of Henri IV found during the excavations. According to Gérard Benéteau, four of the five menhirs have anthropomorphic characteristics. The granite menhirs were regularly dressed by bush-hammering, whereas the sandstone menhir received a coarser treatment. Petrographic study confirmed the local origin of the granite slabs, but the nearest sandstone source lies 2,5 km further south. The wedging stones are of varied kinds (quartz, aplite, limestone) and come from outcrops or from the beds of nearby streams.

Alignment G2 bis lies about 45 m south-west of G2. It was discovered only during the excavation campaign of 2009-2010 and consists of three small menhirs, one of which has anthropomorphic characteristics.

Alignment G3 is the westernmost. It consists of five granite blocks, the tallest 3 m high and the smallest 0,60 m. This alignment has not been excavated.